Abstract
Throughout a 13 year period, the Throughfall Displacement Experiment sustained both increased (+33; wet) and decreased (-33%; dry) throughfall into an upland oak forest in Tennessee. Organic (O) horizon carbon (C) stocks were measured at several occasions before, during and after the experiment and mineral soil C stocks before and after the experiment. In the O horizon, higher C stocks were observed in the dry treatment compared to the ambient and wet, attributable to a combination of enhanced litter inputs and reduced decomposition. No precipitation treatment effects on mineral soil C stocks were found to a depth of 60 cm. Conversely, long-term reductions in surface mineral soil C stocks were surprisingly high for all treatments (3.5-2.7% C in the 0-15 cm layer and from 0.6 to 0.5% in the 15-30 cm layer) over the duration of the experiment. A clear explanation for this temporal trend in C storage was not readily apparent.
Original language | English |
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Pages (from-to) | 151-161 |
Number of pages | 11 |
Journal | Biogeochemistry |
Volume | 89 |
Issue number | 2 |
DOIs | |
State | Published - Jun 2008 |
Funding
Acknowledgements We acknowledge support from the U.S. Department of Energy (DOE), OYce of Science, Biological and Environmental Research (BER) program as part of the Program for Ecosystem Research (PER). Oak Ridge National Laboratory is managed by UT-Battelle, LLC, for the DOE under contract DE-AC05-00OR22725.
Funders | Funder number |
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OYce of Science | |
U.S. Department of Energy | |
Biological and Environmental Research | |
Oak Ridge National Laboratory | DE-AC05-00OR22725 |
Keywords
- Forest soils
- Precipitation
- Soil organic carbon